1 | subroutine largescale(ngrid,nlayer,nq,ptimestep, pplev, pplay, & |
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2 | pt, pq, pdt, pdq, pdtlsc, pdqvaplsc, pdqliqlsc, rneb) |
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3 | |
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4 | |
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5 | ! to use 'getin' |
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6 | ! use ioipsl_getincom |
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7 | use ioipsl_getincom_p |
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8 | use watercommon_h, only : RLVTT, RCPD, RVTMP2, & |
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9 | T_h2O_ice_clouds,T_h2O_ice_liq,Psat_waterDP,Lcpdqsat_waterDP |
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10 | USE tracer_h |
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11 | IMPLICIT none |
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12 | |
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13 | !================================================================== |
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14 | ! |
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15 | ! Purpose |
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16 | ! ------- |
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17 | ! Calculates large-scale (stratiform) H2O condensation. |
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18 | ! |
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19 | ! Authors |
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20 | ! ------- |
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21 | ! Adapted from the LMDTERRE code by R. Wordsworth (2009) |
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22 | ! Original author Z. X. Li (1993) |
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23 | ! |
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24 | !================================================================== |
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25 | |
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26 | INTEGER ngrid,nlayer,nq |
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27 | |
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28 | ! Arguments |
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29 | REAL ptimestep ! intervalle du temps (s) |
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30 | REAL pplev(ngrid,nlayer+1) ! pression a inter-couche |
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31 | REAL pplay(ngrid,nlayer) ! pression au milieu de couche |
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32 | REAL pt(ngrid,nlayer) ! temperature (K) |
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33 | REAL pq(ngrid,nlayer,nq) ! tracer mixing ratio (kg/kg) |
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34 | REAL pdt(ngrid,nlayer) ! physical temperature tenedency (K/s) |
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35 | REAL pdq(ngrid,nlayer,nq)! physical tracer tenedency (K/s) |
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36 | REAL pdtlsc(ngrid,nlayer) ! incrementation de la temperature (K) |
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37 | REAL pdqvaplsc(ngrid,nlayer) ! incrementation de la vapeur d'eau |
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38 | REAL pdqliqlsc(ngrid,nlayer) ! incrementation de l'eau liquide |
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39 | REAL rneb(ngrid,nlayer) ! fraction nuageuse |
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40 | |
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41 | |
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42 | ! Options du programme |
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43 | REAL, SAVE :: ratqs ! determine largeur de la distribution de vapeur |
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44 | !$OMP THREADPRIVATE(ratqs) |
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45 | |
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46 | ! Variables locales |
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47 | REAL CBRT |
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48 | EXTERNAL CBRT |
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49 | INTEGER i, k , nn |
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50 | INTEGER,PARAMETER :: nitermax=5000 |
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51 | DOUBLE PRECISION,PARAMETER :: alpha=.1,qthreshold=1.d-8 |
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52 | ! JL13: if "careful, T<Tmin in psat water" appears often, you may want to stabilise the model by |
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53 | ! decreasing alpha and increasing nitermax accordingly |
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54 | DOUBLE PRECISION zt(ngrid), zq(ngrid) |
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55 | DOUBLE PRECISION zcond(ngrid),zcond_iter |
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56 | DOUBLE PRECISION zdelq(ngrid) |
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57 | DOUBLE PRECISION zqs(ngrid), zdqs(ngrid) |
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58 | DOUBLE PRECISION local_p,psat_tmp,dlnpsat_tmp,Lcp |
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59 | |
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60 | ! evaporation calculations |
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61 | REAL dqevap(ngrid,nlayer),dtevap(ngrid,nlayer) |
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62 | REAL qevap(ngrid,nlayer,nq) |
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63 | REAL tevap(ngrid,nlayer) |
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64 | |
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65 | DOUBLE PRECISION zx_q(ngrid) |
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66 | LOGICAL,SAVE :: firstcall=.true. |
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67 | !$OMP THREADPRIVATE(firstcall) |
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68 | |
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69 | |
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70 | IF (firstcall) THEN |
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71 | |
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72 | write(*,*) "value for ratqs? " |
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73 | ratqs=0.2 ! default value |
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74 | call getin_p("ratqs",ratqs) |
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75 | write(*,*) " ratqs = ",ratqs |
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76 | |
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77 | firstcall = .false. |
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78 | ENDIF |
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79 | |
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80 | ! GCM -----> subroutine variables, initialisation of outputs |
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81 | |
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82 | pdtlsc(1:ngrid,1:nlayer) = 0.0 |
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83 | pdqvaplsc(1:ngrid,1:nlayer) = 0.0 |
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84 | pdqliqlsc(1:ngrid,1:nlayer) = 0.0 |
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85 | rneb(1:ngrid,1:nlayer) = 0.0 |
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86 | Lcp=RLVTT/RCPD |
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87 | |
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88 | |
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89 | ! Evaporate cloud water/ice |
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90 | call evap(ngrid,nlayer,nq,ptimestep,pt,pq,pdq,pdt,dqevap,dtevap,qevap,tevap) |
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91 | ! note: we use qevap but not tevap in largescale/moistadj |
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92 | ! otherwise is a big mess |
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93 | |
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94 | |
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95 | ! Boucle verticale (du haut vers le bas) |
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96 | DO k = nlayer, 1, -1 |
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97 | |
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98 | zt(1:ngrid)=pt(1:ngrid,k)+(pdt(1:ngrid,k)+dtevap(1:ngrid,k))*ptimestep |
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99 | zq(1:ngrid)=qevap(1:ngrid,k,igcm_h2o_vap) !liquid water is included in qevap |
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100 | |
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101 | ! Calculer la vapeur d'eau saturante et |
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102 | ! determiner la condensation partielle |
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103 | DO i = 1, ngrid |
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104 | |
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105 | local_p=pplay(i,k) |
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106 | if(zt(i).le.15.) then |
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107 | print*,'in lsc',i,k,zt(i) |
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108 | ! zt(i)=15. ! check too low temperatures |
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109 | endif |
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110 | call Psat_waterDP(zt(i),local_p,psat_tmp,zqs(i)) |
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111 | |
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112 | zdelq(i) = MAX(MIN(ratqs * zq(i),1.-zq(i)),1.d-12) |
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113 | rneb(i,k) = (zq(i)+zdelq(i)-zqs(i)) / (2.0*zdelq(i)) |
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114 | if (rneb(i,k).lt.0.) then !no clouds |
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115 | |
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116 | rneb(i,k)=0. |
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117 | zcond(i)=0. |
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118 | |
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119 | else if ((rneb(i,k).gt.0.99).or.(ratqs.lt.1.e-6)) then !complete cloud cover, we start without evaporating |
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120 | rneb(i,k)=1. |
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121 | zt(i)=pt(i,k)+pdt(i,k)*ptimestep |
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122 | zx_q(i) = pq(i,k,igcm_h2o_vap)+pdq(i,k,igcm_h2o_vap)*ptimestep |
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123 | dqevap(i,k)=0. |
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124 | ! iterative process to stabilize the scheme when large water amounts JL12 |
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125 | zcond(i) = 0.0d0 |
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126 | Do nn=1,nitermax |
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127 | call Psat_waterDP(zt(i),local_p,psat_tmp,zqs(i)) |
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128 | call Lcpdqsat_waterDP(zt(i),local_p,psat_tmp,zqs(i),zdqs(i),dlnpsat_tmp) |
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129 | zcond_iter = alpha*(zx_q(i)-zqs(i))/(1.d0+zdqs(i)) |
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130 | !zcond can be negative here |
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131 | zx_q(i) = zx_q(i) - zcond_iter |
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132 | zcond(i) = zcond(i) + zcond_iter |
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133 | zt(i) = zt(i) + zcond_iter*Lcp |
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134 | if (ABS(zcond_iter/alpha/zqs(i)).lt.qthreshold) exit |
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135 | ! if (ABS(zcond_iter/alpha).lt.qthreshold) exit |
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136 | if (nn.eq.nitermax) print*,'itermax in largescale' |
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137 | End do ! niter |
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138 | zcond(i)=MAX(zcond(i),-(pq(i,k,igcm_h2o_ice)+pdq(i,k,igcm_h2o_ice)*ptimestep)) |
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139 | |
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140 | else !standard case |
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141 | |
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142 | zx_q(i) = (zq(i)+zdelq(i)+zqs(i))/2.0d0 !water vapor in cloudy sky |
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143 | ! iterative process to stabilize the scheme when large water amounts JL12 |
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144 | zcond(i) = 0.0d0 |
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145 | Do nn=1,nitermax |
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146 | call Lcpdqsat_waterDP(zt(i),local_p,psat_tmp,zqs(i),zdqs(i),dlnpsat_tmp) |
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147 | zcond_iter = MAX(0.0d0,alpha*(zx_q(i)-zqs(i))/(1.d0+zdqs(i))) |
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148 | !zcond always postive! cannot evaporate clouds! |
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149 | !this is why we must reevaporate before largescale |
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150 | zx_q(i) = zx_q(i) - zcond_iter |
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151 | zcond(i) = zcond(i) + zcond_iter |
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152 | if (ABS(zcond_iter/alpha/zqs(i)).lt.qthreshold) exit |
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153 | ! if (ABS(zcond_iter/alpha).lt.qthreshold) exit |
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154 | zt(i) = zt(i) + zcond_iter*Lcp*rneb(i,k) |
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155 | call Psat_waterDP(zt(i),local_p,psat_tmp,zqs(i)) |
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156 | if (nn.eq.nitermax) print*,'itermax in largescale' |
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157 | End do ! niter |
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158 | |
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159 | Endif |
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160 | |
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161 | zcond(i) = zcond(i)*rneb(i,k)/ptimestep ! JL12 |
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162 | |
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163 | ENDDO |
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164 | |
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165 | ! Tendances de t et q |
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166 | pdqvaplsc(1:ngrid,k) = dqevap(1:ngrid,k) - zcond(1:ngrid) |
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167 | pdqliqlsc(1:ngrid,k) = - pdqvaplsc(1:ngrid,k) |
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168 | pdtlsc(1:ngrid,k) = pdqliqlsc(1:ngrid,k)*real(Lcp) |
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169 | |
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170 | Enddo ! k= nlayer, 1, -1 |
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171 | |
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172 | |
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173 | end |
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